Difference between revisions of "Sapping"
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| − | Sapping is a type of erosion where the ground seems to have collapsed into wide valleys. Steep-sided U-shaped valleys of fairly uniform width with box-like, "theater-shaped" headwalls are characteristic of sapping. <ref>Kocher, R. and J. Piper. 1986. Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys. Journal of Geophysical Research. volume = 91. Issue = B13|pages = 175–192.</ref> Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. <ref Rosenberry , | + | Sapping is a type of erosion where the ground seems to have collapsed into wide valleys. Steep-sided U-shaped valleys of fairly uniform width with box-like, "theater-shaped" headwalls are characteristic of sapping. <ref>Kocher, R. and J. Piper. 1986. Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys. Journal of Geophysical Research. volume = 91. Issue = B13|pages = 175–192.</ref> Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. <ref Rosenberry , D. Ground-water Sapping and the Generation of Natural Ampitheaters. University of Colorado websit </ref> |
Valleys made by sapping occur throughout the world including in England, Colorado, Hawai’i, New Zealand, and other places.<ref> Nash, D. 1996. Groundwater Sapping and Valley Development in the Hackness Hills, North Yorkshire, England. volume = 21. issue = 9. edition 9. pages = 781–795</ref> | Valleys made by sapping occur throughout the world including in England, Colorado, Hawai’i, New Zealand, and other places.<ref> Nash, D. 1996. Groundwater Sapping and Valley Development in the Hackness Hills, North Yorkshire, England. volume = 21. issue = 9. edition 9. pages = 781–795</ref> | ||
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[[File:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]] | [[File:Canyonlands NP18.jpg|thumb|right|300px|The two canyons at center-left in this photo from Canyonlands National Park in Utah have the ''theater-shaped'' heads typical of valley features shaped by groundwater sapping.]] | ||
| − | Many channels have been seen on Mars that look like ones created by groundwater sapping here on Earth.<ref>Gulick, V. 2001. Origin of the Valley Networks on Mars: a Hydrological Perspective. Geomorphology. volume = 37. issue = 3–4. | + | |
| + | Many channels have been seen on Mars that look like ones created by groundwater sapping here on Earth.<ref>Gulick, V. 2001. Origin of the Valley Networks on Mars: a Hydrological Perspective. Geomorphology. volume = 37. issue = 3–4. 41–268</ref> | ||
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==See also== | ==See also== | ||
Revision as of 14:50, 13 August 2021
Sapping is a type of erosion where the ground seems to have collapsed into wide valleys. Steep-sided U-shaped valleys of fairly uniform width with box-like, "theater-shaped" headwalls are characteristic of sapping. [1] Sapping is caused by water in the ground moving laterally until it eventually seeps out and creates its ampitheater-like shape. Cite error: Invalid <ref> tag;
invalid names, e.g. too many
Many channels have been seen on Mars that look like ones created by groundwater sapping here on Earth.[2]
See also
References
- ↑ Kocher, R. and J. Piper. 1986. Morphology of Large Valleys on Hawaii: Evidence for Groundwater Sapping and Comparisons with Martian Valleys. Journal of Geophysical Research. volume = 91. Issue = B13|pages = 175–192.
- ↑ Gulick, V. 2001. Origin of the Valley Networks on Mars: a Hydrological Perspective. Geomorphology. volume = 37. issue = 3–4. 41–268
